Xie Weidong, Wang Meng, Vandeginste Veerle, Chen Si, Yu Zhenghong, Wang Jiyao, Wang Hua, Gan Huajun
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences Wuhan 430074 China
School of Earth Resources, China University of Geosciences Wuhan 430074 China.
RSC Adv. 2022 Sep 13;12(40):25947-25954. doi: 10.1039/d2ra03632k. eCollection 2022 Sep 12.
CO is the main greenhouse gas in Earth's atmosphere, and has been causing global warming since the industrial revolution. Therefore, technologies to mitigate carbon emissions have attracted extensive research. Shale gas reservoirs could serve as potential sequestration space for CO. This paper aims to gain insight in the CO adsorption behavior and mechanism in Longmaxi shale. The micropore filling theory is the best model for CO adsorption in the shale samples with the smallest MSR (Mean Square of Residual). This model fits better than that of the monolayer adsorption and multi-layer adsorption theories. Specifically, micropore filling adsorption mainly occurs in micropores, including the closed end of slit pores, capillary pores, and ink-shaped pores. Molecular layer adsorption mainly occurs in mesopores and macropores, including the open end of slit pores, plate pores, capillary pores, and ink-shaped pores. Moreover, the prediction model of CO storage quantity in deep shale gas reservoirs of China is established. This model shows that 91.5-388.89 × 10 m of CO could in theory be stored in an adsorbed state. CO is mostly stored by an adsorbed state (higher than 95%) and a free state with good security and low leakage risk. The results from this work are of specific interest for global research on CO adsorption characteristics and adsorption mechanisms in different pore structures. Furthermore, it provides certain guidance for geological storage of CO in shale.
二氧化碳是地球大气中的主要温室气体,自工业革命以来一直在导致全球变暖。因此,减少碳排放的技术引起了广泛研究。页岩气藏可作为二氧化碳的潜在封存空间。本文旨在深入了解二氧化碳在龙马溪页岩中的吸附行为和机理。微孔填充理论是剩余平方均值最小的页岩样品中二氧化碳吸附的最佳模型。该模型比单层吸附和多层吸附理论拟合得更好。具体而言,微孔填充吸附主要发生在微孔中,包括狭缝孔的封闭端、毛细管孔和墨水瓶形孔。分子层吸附主要发生在中孔和大孔中,包括狭缝孔的开口端、板孔、毛细管孔和墨水瓶形孔。此外,建立了中国深层页岩气藏二氧化碳储存量预测模型。该模型表明,理论上可吸附储存91.5 - 388.89×10立方米的二氧化碳。二氧化碳大多以吸附态储存(高于95%),且以游离态储存时安全性好、泄漏风险低。这项工作的结果对于全球不同孔隙结构中二氧化碳吸附特性和吸附机理的研究具有特殊意义。此外,它为页岩中二氧化碳的地质封存提供了一定指导。